Miller indices are the universal language crystallographers use to describe crystal planes—and if you're studying crystallography, you'll encounter them constantly. Whether you're interpreting X-ray diffraction patterns, predicting material properties, or analyzing crystal symmetry, Miller indices provide the foundation for communicating precisely about three-dimensional crystal structures. The concepts here connect directly to reciprocal space, Bragg's law, structure factor calculations, and symmetry operations—all core topics you'll be tested on.
Don't just memorize that Miller indices are written as (hkl). Focus on understanding why we use reciprocals of intercepts, how these indices relate to the reciprocal lattice, and what they tell us about interplanar spacing and diffraction. When exam questions ask you to calculate indices or interpret diffraction data, you're really being tested on whether you understand the geometric and mathematical principles behind the notation.
Fundamentals: What Miller Indices Are and How to Find Them
Miller indices translate the geometric relationship between a crystal plane and the lattice axes into a compact, standardized notation using reciprocals of axis intercepts.
Definition of Miller Indices
Three integers (h, k, l) represent the orientation of any crystal plane relative to the unit cell axes—this is the foundation of all crystallographic plane notation
Reciprocal relationship—the indices are inversely proportional to where the plane intercepts each axis, which connects directly to reciprocal lattice concepts
Universal convention allows crystallographers worldwide to describe identical planes without ambiguity, essential for comparing structures across literature
Notation and Representation (hkl)
Parentheses (hkl) denote a specific plane, while curly braces {hkl} represent all symmetry-equivalent planes—know this distinction for exams
Negative indices use a bar notation (e.g., 1ˉ for -1), written as (hˉkl) to indicate intercepts on negative axis directions
Lowest integer form is always used—indices like (2, 4, 2) must be reduced to (1, 2, 1) to maintain the convention
Calculation of Miller Indices
Step 1: Find intercepts of the plane with the three crystallographic axes, expressed as multiples of lattice parameters
Step 2: Take reciprocals of these intercepts—a plane parallel to an axis has an intercept at infinity, giving a reciprocal of zero
Step 3: Clear fractions and reduce to the smallest integers; for example, intercepts of (1, ½, ∞) become reciprocals (1, 2, 0), giving indices (120)
Compare: A plane with intercepts (1, 1, 1) vs. (2, 2, 2)—both yield Miller indices (111) because we always reduce to lowest integers. The indices describe orientation, not the specific plane's distance from the origin. If asked to distinguish parallel planes, you'll need interplanar spacing instead.
Connecting to Physical Space: Planes and Spacing
Miller indices don't just label planes—they encode geometric information about how planes are oriented and spaced within the crystal lattice.
Relationship to Crystal Planes
Each (hkl) set defines a family of parallel planes with identical orientation and uniform spacing throughout the infinite lattice
Higher indices mean steeper angles—a (311) plane cuts across the unit cell more sharply than a (100) plane, which lies flat against one face
Visualization technique: sketch where the plane would intersect axes at a/h, b/k, and c/l to see the plane's orientation in real space
Interplanar Spacing
The d-spacing is the perpendicular distance between adjacent parallel planes of the same Miller indices—this is what X-rays actually measure
Cubic system formula: dhkl=h2+k2+l2a, where a is the lattice parameter—memorize this relationship
Inverse relationship: higher Miller indices correspond to smaller d-spacings, meaning more closely packed planes and higher-angle diffraction peaks
Compare: The (100) plane in a cubic crystal has d=a, while (111) has d=a/3≈0.577a. This explains why (111) peaks appear at higher 2θ angles in diffraction patterns—Bragg's law directly connects d-spacing to diffraction angle.
Reciprocal Space: Where Miller Indices Live Naturally
The reciprocal lattice transforms the periodic real-space crystal into a representation where each point corresponds to a set of crystal planes—and Miller indices become coordinates.
Reciprocal Lattice Concept
Each reciprocal lattice point at position (h, k, l) represents the entire family of real-space planes with those Miller indices—this is the key conceptual bridge
Vector magnitude of the reciprocal lattice vector Ghkl equals 2π/dhkl, directly encoding interplanar spacing information
Diffraction condition: X-ray diffraction occurs when the scattering vector equals a reciprocal lattice vector—this is why Miller indices appear in every diffraction analysis
Significance in X-ray Diffraction
Bragg peaks are labeled by (hkl) because each peak corresponds to diffraction from planes with those Miller indices—the indices are the peak identification
Peak intensity depends on the structure factorFhkl, which sums atomic scattering contributions based on atom positions relative to (hkl) planes
Systematic absences occur when certain (hkl) combinations give zero intensity due to destructive interference—these reveal lattice centering and symmetry
Compare: In a body-centered cubic (BCC) lattice, (100) reflections are absent while (110) reflections appear; in face-centered cubic (FCC), (100) and (110) are both absent but (111) appears. Exam questions often ask you to predict which peaks are missing based on lattice type—use the selection rules: BCC requires h+k+l = even; FCC requires h, k, l all odd or all even.
Symmetry and Special Systems
Crystal symmetry constrains which Miller indices are truly distinct and requires modified notation for non-cubic systems.
Symmetry Considerations
Equivalent planes related by symmetry operations share physical properties—the family notation {hkl} groups all symmetry-equivalent (hkl) planes together
Multiplicity counts how many equivalent planes exist; for example, {100} in a cubic system includes (100), (010), (001), and their negatives—six planes total
Selection rules for diffraction arise from symmetry: certain (hkl) combinations produce zero intensity due to systematic cancellation from symmetry-related atoms
Zone Axis and Zone Equation
A zone axis [uvw] is a crystallographic direction that lies parallel to the intersection of multiple crystal planes—planes sharing a zone axis form a "zone"
Zone equation: a plane (hkl) belongs to zone [uvw] if hu+kv+lw=0—this relationship is essential for electron diffraction pattern analysis
Practical use: when viewing a crystal along a zone axis in electron microscopy, you see diffraction spots only from planes in that zone
Miller-Bravais Indices for Hexagonal Systems
Four-index notation (hkil) captures the unique 6-fold symmetry of hexagonal crystals that three indices cannot elegantly represent
Redundancy constraint: the third index always satisfies i=−(h+k), so it carries no independent information but clarifies equivalent planes
Conversion: to convert from (hkl) to (hkil), keep h and k, calculate i=−(h+k), and keep l—this preserves all orientation information
Compare: In hexagonal systems, the planes (101ˉ0), (011ˉ0), and (1ˉ100) are symmetry-equivalent—the four-index notation makes this equivalence visually obvious (all have the same form), while three-index notation would obscure the relationship. Use Miller-Bravais indices whenever you're working with hexagonal materials like graphite, zinc, or many ceramics.
Quick Reference Table
Concept
Key Points
Index Calculation
Reciprocals of intercepts → clear fractions → reduce to lowest integers
Notation Conventions
(hkl) = specific plane, {hkl} = equivalent planes, [uvw] = direction
Interplanar Spacing (Cubic)
dhkl=a/h2+k2+l2
Reciprocal Lattice
Point (hkl) represents plane family; ∥G∥=2π/d
Diffraction Connection
Peak positions from Bragg's law + d-spacing; intensities from structure factor
Systematic Absences
BCC: h+k+l = even; FCC: h,k,l all odd or all even
Zone Equation
Plane (hkl) in zone [uvw] if hu+kv+lw=0
Hexagonal Systems
Use (hkil) with i=−(h+k) to show 6-fold symmetry
Self-Check Questions
A plane intercepts the crystallographic axes at 2a, 3b, and ∞ (parallel to c). What are its Miller indices, and what does the zero index physically mean?
Compare the interplanar spacings of (110) and (111) planes in a cubic crystal with lattice parameter a. Which produces a diffraction peak at a higher 2θ angle, and why?
You observe that (100), (110), and (211) reflections are all absent in an X-ray pattern, but (200) and (222) appear. What type of lattice centering does this suggest?
Why do hexagonal crystals use four Miller-Bravais indices when only three are mathematically independent? Give an example of how this notation clarifies symmetry relationships.
If you're analyzing an electron diffraction pattern taken along the [001] zone axis, which of the following planes could contribute to the pattern: (100), (110), (111), (210)? Use the zone equation to justify your answer.